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Updated: Jan 14, 2026

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Methane Hydrate Crystallization on Sessile Water Droplets
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水の液体-液体遷移に関する証拠の再考:断熱実験が明らかにするもの
Rajat Kumar1, Ingrid de Almeida Ribeiro1, Debdas Dhabal2
1Department of Chemistry, The University of Utah, Salt Lake City, Utah 84112-0850, USA.
The Journal of chemical physics
|January 13, 2026
まとめ
水の液体-液体遷移は、ナノスケールのドメインにより構造因子S(q)に単一のピークを示します。主要なシグネチャはピーク分裂ではなく、観測される相関長ξであり、実験的矛盾を解決します。
背景:
- 過冷却水における液体-液体遷移(LLT)の存在は、長年の議論の的となっています。
- 実験的研究では、断熱中の構造因子S(q)における2つのピークに基づいて、液体-液体の共存を示唆しています。
- この解釈は、液体-液体臨界点(LLCP)を超える共存に関する理論的予測と矛盾します。
結論:
- S(q)ピーク分裂ではなく、低qにおける観測される相関長ξの進化が、水におけるLLTの主要な構造マーカーです。
- 実験的シグネチャは、特定の圧力低下プロファイルとそれに続くξの成長および減衰によって説明できます。
- 本研究は、LLCPの位置と観察された構造的シグネチャの間の矛盾を解決し、水のLLTの性質を明らかにします。
キーワード:
liquid-liquid transitionwaterstructure factorcorrelation lengthdecompression experimentssupercooled watercritical pointさらに関連する動画
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